Available with Image Server

The Surface Parameters tool calculates parameters of a raster surface such as aspect, slope, and curvature using geodesic methods.

The output is a hosted imagery layer.

Learn how Surface Parameters works

## Examples

The Surface Parameters tool can be used in the following scenarios:

- Calculate aspect and slope using geodesic methods.
- Calculate different types of curvatures using geodesic methods. For example, you can calculate tangential curvature, which characterizes topographic convergence and divergence of flow across the surface.

## Usage notes

Surface Parameters includes configurations for input layer, surface parameter settings, and result layer.

### Input layer

The Input layer group includes the following parameter:

Input surface raster is the surface raster that will be used for calculation.

If a z-unit is available in the vertical coordinate system of the input raster, it will be applied automatically. If the z-unit is undefined, Meter will be used by default.

The Optional layers group includes the following parameters:

The Input analysis mask raster or features specifies the locations where the analysis will occur. It can be a raster or feature. You can choose a layer using the Layer button or use the Draw input features button to create a sketch layer to use as the input.

If the input is a feature, it can be point, line, or polygon type.

If the input is a raster, it can be integer or floating-point type. When the input mask data is a raster, the analysis will occur at locations that have a valid value, including zero. Cells that are NoData in the mask input will be NoData in the output.

When the Input surface raster and the Input analysis mask raster or features parameter values are of the same cell size and the cells are aligned, they will be used directly in the tool. They will not be resampled internally during the tool operation.

If the cell size is different, the output cell size will be the maximum of the inputs, and the Input surface raster value will be used internally as the snap raster. If the cell size is the same but the cells are not aligned, the Input surface raster value will be used internally as the snap raster. Either of these cases will cause an internal resampling before the extraction operation is performed. For additional information, see the Cell size and Snap raster environment topics.

The Input analysis mask raster or features will take priority over the Mask environment setting.

### Surface parameter settings

The Surface parameter settings group includes the following parameters:

Parameter type specifies the surface parameter type that will be computed.

Each available surface parameter type is calculated on a cell-by-cell basis by fitting a local surface around a target cell. The units of all curvature type outputs will be the reciprocal (the square of the reciprocal for Gaussian curvature) of the x,y-units of the output coordinate system. The available options are as follows:

- Slope—The rate of change in elevation, the first derivative of a DEM, will be computed. The range of values from the slope output depends on the unit specified for the Slope measurement parameter. This is the default.
- Aspect—The downslope direction of the maximum rate of change for each cell will be computed. The output represents the compass direction that the downhill slope faces for each location. It is expressed in positive degrees from 0 to 360, measured clockwise from north.
- Mean Curvature—The overall curvature of the surface will be measured. It is computed as the average of the minimum and maximum curvature. This curvature describes the intrinsic convexity or concavity of the surface, independent of direction or gravity influence. High positive values indicate areas of maximum denudation, and high negative values indicate areas of maximum accumulation (Minár et al., 2020).
- Tangential (normal contour) Curvature—The geometric normal curvature perpendicular to the slope line, tangent to the contour line will be measured. This curvature is typically applied to characterize the convergence or divergence of flow across the surface. Positive values indicate areas of diverging surface flow. Negative tangential curvatures indicate areas of converging surface flow. A positive tangential (normal contour) curvature indicates that the surface is convex at that cell perpendicular to the direction of the slope. A negative curvature indicates that the surface is concave at that cell in the direction perpendicular to the slope. A value of 0 indicates that the surface is flat.
- Profile (projected contour) Curvature—The geometric normal curvature along the slope line will be measured. This curvature is typically applied to characterize the acceleration and deceleration of flow down the surface. Positive values indicate areas of acceleration of surface flow and erosion. Negative profile curvature indicates areas of slowing surface flow and deposition. A positive profile (normal slope line) curvature indicates that the surface is convex at that cell in the direction of the slope. A negative curvature indicates that the surface is concave at that cell in that same direction. A value of 0 indicates that the surface is flat.
- Plan (projected contour) Curvature—The curvature along contour lines will be measured.
- Contour geodesic torsion—The rate of change in slope angle along contour lines will be measured.
- Gaussian curvature—The overall curvature of the surface will be measured. It is computed as the product of the minimum and maximum curvature. Positive values indicate that the surface is convex at that cell, and negative values indicate that it is concave. A value of 0 indicates that the surface is flat.
- Casorati curvature—The general curvature of the surface will be measured. It can be zero or any other positive number. It can be zero or always positive. High positive values indicate areas of sharp bending in multiple directions.

Slope measurement specifies the measurement units that will be used for the output slope raster.

This parameter is only available if the Parameter type parameter is set to Slope. The available options are as follows:

- Degrees—The range of slope values is 0 to 90 degrees.
- Percent rise—The range is 0 to essentially infinity. A flat surface is 0 percent, a 45 degree surface is 100 percent, and as the surface becomes more vertical, the percent rise becomes increasingly larger.

Project geodesic azimuths specifies whether geodesic azimuths will be projected to correct the angle distortion caused by the output spatial reference.

This parameter is only available if the Parameter type parameter is set to Aspect.

- Unchecked—Geodesic azimuths will not be projected. This is the default.
- Checked—Geodesic azimuths will be projected. In this case, north is always represented by 360 degrees and azimuths will be projected to correct the distortion caused by a nonconformal Output Coordinate System environment setting. These angles can be used to accurately locate points along the steepest downhill slope. Check the Project geodesic azimuths parameter if you are using the Surface Parameters tool output as a back direction input for the Input back direction raster parameter for a tool in the Use proximity toolset.

Use equatorial aspect specifies whether aspect will be measured from a point on the equator or from the north pole.

This parameter is only available if the Parameter type parameter is set to Aspect.

- Unchecked—Aspect will be measured from the north pole. This is the default.
- Checked—Aspect will be measured from a point along the equator to correct for the skewing of direction that occurs when approaching the poles. This parameter ensures that the north-south and east-west axes are perpendicular to each other. Use this option if the terrain is near the north or south pole.

Local surface type specifies the type of surface function that will be fitted around the target cell. The available options are as follows:

Quadratic—A quadratic surface function will be fitted to the neighborhood cells. This surface function does not fit the neighborhood cells exactly, which is recommended for most data and applications. This is the default.

The quadratic surface minimizes the impact of noise in the input surface raster, which is especially important when computing curvature.

Use this option when specifying a neighborhood size through the Neighborhood distance parameter that is larger than the cell size and when using the adaptive neighborhood option.

Biquadratic—A biquadratic surface function will be fitted to the neighborhood cells.

This option is suitable for a highly accurate input surface.

If the neighborhood distance is larger than the input raster cell size, the accuracy advantages of the biquadratic surface type will be lost. Leave the neighborhood distance as the default (equal to the cell size).

Neighborhood distance is the distance from the target cell center from which the output will be calculated. It determines the neighborhood size.

The default value is the input raster cell size, resulting in a 3 by 3 neighborhood. It cannot be less than the input raster cell size. If a neighborhood distance is specified that does not result in an odd interval of the cell size, it will round up to the next interval of the cell size. In addition, the largest neighborhood distance is equal to 7 times the cell size, resulting in a 15 by 15 cell window. Any specified distance that is larger than 7 times the cell size will always result in using a 15 by 15 cell window.

A smaller neighborhood distance captures more local variability in the landscape, characteristics of smaller landscape features. With high resolution elevation data, larger distances may be more appropriate.

Use adaptive neighborhood specifies whether neighborhood distance will vary with landscape changes. The neighborhood distance will shrink if there is too much variability in the calculation window. The maximum distance is determined by the value of the Neighborhood distance parameter.

The minimum distance is the input raster cell size.

- Unchecked—A single (fixed) neighborhood distance will be used at all locations. This is the default.
- Checked—An adaptive neighborhood distance will be used at all locations.

Z unit specifies the linear unit of vertical z-values.

It is defined by a vertical coordinate system, if it exists. If a vertical coordinate system does not exist, the z unit should be defined from the unit list to ensure correct geodesic computation. The default is Meter. The available linear units are Inch, Foot, Yard, Mile US, Nautical mile, Millimeter, Decimeter, Centimeter, Meter, and Kilometer.

### Result layer

The Result layer group includes the following parameters:

Output raster name is the name of the raster that contains the specified surface parameter type values.

The name must be unique. If a layer with the same name already exists in your organization, the tool will fail and you will be prompted to use a different name.

- Save in folder specifies the name of a folder in My content where the result will be saved.

## Environments

Analysis environment settings are additional parameters that affect a tool's results. You can access the tool's analysis environment settings from the Environment settings parameter group.

This tool honors the following analysis environments:

- Output coordinate system
- Processing extent
##### Note:

The default processing extent in Map Viewer is Full extent. This default is different from Map Viewer Classic in which Use current map extent is enabled by default.

- Snap raster
- Cell size
- Mask
- Parallel processing factor

## Output

The output is one output raster with the specified surface parameters type values.

## Usage requirements

This tool requires the following licensing and configurations:

- Creator or GIS Professional user type
- Publisher or Administrator role, or an equivalent custom role
- ArcGIS Image Server configured for raster analysis

## References

- James D.E., M.D. Tomer, S.A. Porter. 2014. "Trans-scalar landform segmentation from high-resolution digital elevation models." Poster presented at: ESRI Annual Users Conference; July 2014; San Diego, California.
- Minár, J., Evans, I. S., & Jenčo, M. 2020. "A comprehensive system of definitions of land surface (topographic) curvatures, with implications for their application in geoscience modelling and prediction". Earth-Science Reviews, 103414. https://doi.org/10.1016/j.earscirev.2020.103414

## Resources

Use the following resources to learn more:

- How Surface Parameters works
- Surface Parameters in ArcGIS REST API
- Surface Parameters in ArcGIS Pro with the Raster Analysis extension
- Surface Parameters in ArcGIS Pro with the Spatial Analyst extension